Walpole, B. P.
This Thesis presents an account of the
geology of the Lower Proterozoic rocks which
occupy the Pine Creek Geosyncline, and attempts
to trace the evolution of the geosyncline by a
reconstruction of the sequence of deposition of
the sediments; by relating different facies
assemblages to structural units developed in the
geosynolinal tract; and by a brief consideration
of the igneous rocks, which, together with the
sediments, make up the geosynclinal pile. The
geosyncline is discussed as...[Show more]
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